CF油田火山热液流体活动及其对碳酸盐岩储层的改造作用
|
摘要
为探讨CF油田热液活动对古生界碳酸盐岩储层的影响,对岩心、薄片、扫描电镜、阴极发光、碳氧锶同位素、流体包裹体等进行了综合分析。研究认为:碳酸盐岩储层中存在典型的热褪色、细密不规则诱导缝,发育鞍形白云石、硅质结核、自生石英等典型热液矿物;受热液影响的方解石阴极发光下发亮橘黄色光、δ18O值异常低、87Sr/86Sr值异常高,盐水包裹体均一温度明显高于地层温度;富含Mg~(2+)的酸性岩浆热液流体沿断裂涌入地层,促使围岩发生白云石化作用,产生大量的晶间孔,同时溶蚀碳酸盐岩,形成大量的溶蚀孔隙;受热液流体作用影响形成的诱导缝可进一步沟通储集空间,改善了储层的渗透性,提升了碳酸盐岩储层储集性能。
In order to find out the influence of the hydrothermal activities on Paleozoic carbonate reservoir in CF Oilfield,the comprehensive analyses on the core,thin section,scanning electron microscope,cathodeluminescence,carbon-oxygen-strontium isotopes,fluid inclusion and so on were engaged. The study shows that there are typical thermal fading,fine and irregular induced fractures in the carbonate reservoirs,and the typical hydrothermal minerals such as saddle dolomite,siliceous nodules,authigenic quartz and so forth have been found; under the influence of the hydrothermal fluid,the calcite glowing orange yellow,low-value δ18O,high-content87Sr/86 Sr and obviously high homogenized temperature of the brine inclusions than the temperature of the surrounding rock; Mg2+-enriched acidic magmatic hydrothermal fluids flow into the formations along the faults and cause dolomitization of the surrounding rocks,thus result in a large number of intergranular pores,while dissolve the carbonate rocks and form a large number of dissolved pores; the induced fractures constructed by the hydrothermal fluid can further communicate the reservoir space and greatly improve the reservoir permeability,finally the accumulating performance of the carbonate reservoir has been enhanced.
In order to find out the influence of the hydrothermal activities on Paleozoic carbonate reservoir in CF Oilfield,the comprehensive analyses on the core,thin section,scanning electron microscope,cathodeluminescence,carbon-oxygen-strontium isotopes,fluid inclusion and so on were engaged. The study shows that there are typical thermal fading,fine and irregular induced fractures in the carbonate reservoirs,and the typical hydrothermal minerals such as saddle dolomite,siliceous nodules,authigenic quartz and so forth have been found; under the influence of the hydrothermal fluid,the calcite glowing orange yellow,low-value δ18O,high-content87Sr/86 Sr and obviously high homogenized temperature of the brine inclusions than the temperature of the surrounding rock; Mg2+-enriched acidic magmatic hydrothermal fluids flow into the formations along the faults and cause dolomitization of the surrounding rocks,thus result in a large number of intergranular pores,while dissolve the carbonate rocks and form a large number of dissolved pores; the induced fractures constructed by the hydrothermal fluid can further communicate the reservoir space and greatly improve the reservoir permeability,finally the accumulating performance of the carbonate reservoir has been enhanced.
引文
[1]李欣,闫伟鹏,崔周旗,等.渤海湾盆地潜山油气藏勘探潜力与方向[J].石油实验地质,2012,34(2):140-145.LI Xin,YAN Weipeng,CUI Zhouqi,et al. Prospecting potential and targets of buried-hill oil and gas reservoirs in Bohai Bay Basin[J]. Petroleum Geology&Experiment, 2012, 34(2):140-145.
[2]杨明慧.渤海湾盆地潜山多样性及其成藏要素比较分析[J].石油与天然气地质,2008,29(5)623-632.YANG Minghui. Diversity of buried-hills and comparison of their hydrocarbon-pooling factors in Bohai Bay Basin[J]. Oil&Gas Geology,2008,29(5)623-632.
[3]吴伟涛,高先志,李理,等.渤海湾盆地大型潜山油气藏形成的有利因素[J].特种油气藏,2015,22(2):22-28.WU Weitao, GAO Xianzhi, LI Li,et al. Favorable conditions formed in large-scale buried-hill reservoir in Bohai Bay Basin[J].Special Oil and Gas Reservoirs,2015,22(2):22-28.
[4]吴永平,肖敦清,于俊利.黄骅坳陷孔西潜山特殊油气藏的发现[J].特种油气藏,1998,22(2):1-6.WU Yongping,XIAO Dunqing,YU Junli. Discovery of special reservoir of Kongxi buried hill in Huanghua Depression[J]. Special Oil and Gas Reservoirs,1998,22(2):1-6.
[5]赵贤正,金凤鸣,王权,等.渤海湾盆地牛东1超深潜山高温油气藏的发现及其意义[J].石油学报,2011,32(6):915-927.ZHAO Xianzheng,JIN Fengming,WANG Quan,et al. Niudong 1ultra-deep and ultra-high temperature subtle buried hill field in Bohai Bay Basin:Discovery and significance[J]. Acta Petrolei Sinica,2011,32(6):915-927.
[6]马立驰,王永诗,吕建波.济阳坳陷下古生界潜山内幕油气藏勘探[J].油气地质与采收率,2004,11(1):26-29.MA Lichi,WANG Yongshi,LJianbo. Exploration on internal pool of buried hill in lower Palaeozoic group of Jiyang Depression[J].Petroleum Geology and Recovery Efficiency, 2004, 11(1):26-29.
[7]王少鹏,杨庆红,郭铁恩,等.渤海海域CF油田古生界碳酸盐岩潜山储层特征[J].大庆石油地质与开发,2014,33(2):16-21.WANG Shaopeng,YANG Qinghong,GUO Tieen,et al. Characteristics of the Paleozoic carbonate buried-hill reservoirs in CF Oilfield of Bohai Sea[J]. Petroleum Geology&Oilfield Development in Daqing,2014,33:(2)16-21.
[8]于海波,王德英,牛成民,等.渤海海域渤南低凸起碳酸盐岩潜山储层特征及形成机制[J].石油实验地质,2015,37(2):150-157.YU Haibo,WANG Deying,NIU Chengmin,et al. Characteristics and formation mechanisms of buried hill carbonate reservoirs in Bonan Low Uplift, Bohai Bay[J]. Petroleum Geology&Experiment,2015,37(2):150-157.
[9]陈丽祥,牛成民,李慧勇,等.渤海湾盆地渤中21-2构造碳酸盐岩储层发育特征及其控制因素[J].油气地质与采收率,2016,23(2):16-21.CHEN Lixiang,NIU Chengmin,LI Huiyong,et al. Carbonate reservoir characteristics and its controlling factors in Bozhong 21-2Structure,Bohai Bay Basin[J]. Petroleum Geology and Recovery Efficiency,2016,23(2):16-21.
[10]王粤川,韦阿娟,高坤顺,等.渤海海域沙垒田凸起西北部奥陶系碳酸盐岩储层发育主控因素与分布预测[J].海相油气地质,2016,21(2):13-21.WANG Yuechuan,WEI Ajuan,GAO Kunshun,et al. Development controlling factors and distribution predication of Ordovician carbonate reservoirs in the northwestern part of Shaleitian Arch,Offshore Bohai Sea[J]. Marine Origin Petroleum Geology,2016,21(2):13-21.
[11]赵国祥,王清斌,杨波,等.渤中凹陷奥陶系深埋环境下碳酸盐岩溶蚀成因分析[J].天然气地球科学,2016,27(1):111-120.ZHAO Guoxiang,WANG Qingbin,YANG Bo,ea al. Dissolution mechanism analysis of Ordovician carbonates under burial environment of Bozhong Sag,Bohai Sea area[J]. Natural Gas Geoscience,2016,27(1):111-120.
[12]金之钧,朱东亚,胡文瑄,等.塔里木盆地热液活动地质地球化学特征及其对储层影响[J].地质学报,2006,80(2):245-254.JIN Zhijun,ZHU Dongya,HU Wenxuan,et al. Geological and geochemical signatures of hydrothermal activity and their influence on carbonate reservoir beds in the Tarim Basin[J]. Acta Geologica Sinica,2006,80(2):245-254.
[13]朱松柏,王洪峰,王胜军,等.玉北地区深部热液活动的发现及其储层改造意义[J].岩性油气藏,2016,28(3):42-47.ZHU Songbai,WANG Hongfeng,WANG Shengjun,et al. Hydrothermal activities of Ordovician and its significance for alteration to carbonate reservoirs in Yubei area[J]. Lithologic Reservoirs,2016,28(3):42-47.
[14]田雷,崔海峰,冯晓军,等.麦盖提斜坡奥陶系热液溶蚀流体对内幕白云岩储层的改造作用[J].石油与天然气地质,2015,36(3):402-408.TIAN Lei,CUI Haifeng,FENG Xiaojun,et al. Reconstruction effect of the Ordovician hydrothermal dissolution fluid on interior dolomite reservoirs in Maigaiti Slope,Tarim Basin[J]. Oil&Gas Geology,2015,36(3):402-408.
[15]李忠,黄思静,刘嘉庆,等.塔里木盆地塔河奥陶系碳酸盐岩储层埋藏成岩和构造—热流体作用及其有效性[J].沉积学报,2010,28(5):969-979.LI Zhong,HUANG Sijing,LIU Jiaqing,et al. Buried diagenesis,structurally controlled thermal-fluid process and their effect on Ordovician Carbonate Reservoirs in Tahe,Tarim Basin[J]. Acta Sedimentologica Sinica,2010,28(5):969-979.
[16]李辉,李国蓉,罗韵,等.塔河地区奥陶系碳酸盐岩储层深部热液特征分析[J].东北石油大学学报,2014,38(6):12-23.LI Hui,LI Guorong,LUO Yun,et al. Buried Diagenesis,Analysis of characteristics of deep hydrothermal fluids in Ordovician carbonate reservoir in Tahe area[J]. Journal of Northeast Petroleum University,2014,38(6):12-23.
[17]朱东亚,金之钧,孙冬胜,等.南方震旦系灯影组热液白云岩化及其对储层形成的影响研究:以黔中隆起为例[J].地质科学,2014,49(1):161-175.ZHU Dongya,JIN Zhijun,SUN Dongsheng,et al. Hydrothermal dolomitization of Dengying Formation of Sinian in South China and its effect on reservoir formation:An example from Qianzhong Uplift[J]. Chinese Journal of Geology,2014,49(1):161-175.
[18]杨海军,李开开,潘文庆,等.塔中地区奥陶系埋藏热液溶蚀流体活动及其对深部储层的改造作用[J].岩石学报,2012,28(3):783-792.YANG Haijun,LI Kaikai,PAN Wenqing,et al. Burial hydrothermal dissolution fluid activity and its transforming effect on the reservoirs in Ordovician in Central Tarim[J]. Acta Petrologica Sinica,2012,28(3):783-792.
[19]李大伟.新构造运动与渤海湾盆地上第三系油气成藏[J].石油与天然气地质,2004,25(2):170-175.LI Dawei. Neotectonism and Neogene oil and gas pools in Bohai Bay Basin[J]. Oil&Gas Geology,2004,25(2):170-175.
[20]董月霞,周海民,夏文臣.南堡凹陷火山活动与裂陷旋回[J].石油与天然气地质,2000,21(4):24-27.DONG Yuexia, ZHOU Haimin, XIA Wenchen. Volcanic activities and rift-subsidence cycles in Nanpu Sag[J]. Oil&Gas Geology,2000,21(4):24-27.
[21]金之钧,胡文瑄,张刘平,等.深部流体活动及油气成藏效应[M].北京:科学出版社,2007:40-53.JIN Zhijun,HU Wenxuan,ZHANG Liuping,et al. Deep fluid activities and their effectiveness on hydrocarbon generation and accumulation[M]. Beijing:Science Press,2007:40-53.
[22]李庆,胡文瑄,张军涛,等.塔里木盆地西北缘中寒武统硅质岩特征与形成环境[J].矿物学报,2010,30(3):293-303.LI Qing,HU Wenxuan,ZHANG Juntao, et al. Characteristics and formation environment of Middle Cambrian siliconites in Northwestern Margin of Tarim Basin[J]. Acta Mineralogica Sinica,2010,30(3):293-303.
[23]肖波,秦克章,李光明,等.西藏驱龙巨型斑岩Cu-Mo矿床的富S、高氧化性含矿岩浆:来自岩浆成因硬石膏的证据[J].地质学报,2009,83(12):1860-1868.XIAO Bo,QIN Kezhang,LI Guangming, et al. S-rich, highlyoxidized ore-bearing magma in the Qulong giant porphyry-type CuMo deposit in Southern Tibet:Evidence from magmatogenic anhydrite[J]. Acta Geologica Sinica,2009,83(12):1860-1868.
[24]刘丽红,黄思静,王春莲,等.碳酸盐岩中方解石胶结物的阴极发光环带与微量元素构成的关系:以塔河油田奥陶系碳酸盐岩为例[J].海相油气地质,2010,15(1):55-60.LIU Lihong, HUANG Sijing, WANG Chunlian, et al. Cathodoluminescence zonal texture of calcite cement in carbonate rock and its relationship with trace element composition:A case of Ordovician carbonate rock of Tahe Oilfield, Tarim Basin[J].Marine Origin Petroleum Geology,2010,15(1):55-60.
[25]张浩,陈刚,朱玉双,等.柴达木盆地英西地区渐新统热液改造型白云岩的发现与意义[J].地质科技情报,2017,36(1):87-97.ZHANG Hao,CHEN Gang,ZHU Yushuang,et al. Discovery and significance of dolomites altered by hydrothermal fluid in Oligocene reservoirs of the Yingxi Area, Qaidam Basin[J]. Geological Science and Technology Information,2017,36(1):87-97.
[26]黄擎宇.塔里木盆地中央隆起区寒武-奥陶系白云岩化作用及白云岩储层成因研究[D].成都:成都理工大学,2014:48-60.HUANG Qingyu. Dolomitization and origin of the Cambrian-Ordovician dolomite reservoirs in the Central Uplift, Tarim Basin[D]. Chengdu:Chengdu University of Technology,2014:48-60.
[27]杨宁,吕修祥,郑多明.塔里木盆地火成岩对碳酸盐岩储层的改造作用[J].西安石油大学学报(自然科学版),2005,20(4):1-4.YANG Ning,LXiuxiang,ZHENG Duoming. Alteration of the igneous rock on the carbonate reservoir in Tarim Basin[J].Journal of Xi’an Shiyou Universitiy(Natural Science Edition),2005,20(4):1-4.
[2]杨明慧.渤海湾盆地潜山多样性及其成藏要素比较分析[J].石油与天然气地质,2008,29(5)623-632.YANG Minghui. Diversity of buried-hills and comparison of their hydrocarbon-pooling factors in Bohai Bay Basin[J]. Oil&Gas Geology,2008,29(5)623-632.
[3]吴伟涛,高先志,李理,等.渤海湾盆地大型潜山油气藏形成的有利因素[J].特种油气藏,2015,22(2):22-28.WU Weitao, GAO Xianzhi, LI Li,et al. Favorable conditions formed in large-scale buried-hill reservoir in Bohai Bay Basin[J].Special Oil and Gas Reservoirs,2015,22(2):22-28.
[4]吴永平,肖敦清,于俊利.黄骅坳陷孔西潜山特殊油气藏的发现[J].特种油气藏,1998,22(2):1-6.WU Yongping,XIAO Dunqing,YU Junli. Discovery of special reservoir of Kongxi buried hill in Huanghua Depression[J]. Special Oil and Gas Reservoirs,1998,22(2):1-6.
[5]赵贤正,金凤鸣,王权,等.渤海湾盆地牛东1超深潜山高温油气藏的发现及其意义[J].石油学报,2011,32(6):915-927.ZHAO Xianzheng,JIN Fengming,WANG Quan,et al. Niudong 1ultra-deep and ultra-high temperature subtle buried hill field in Bohai Bay Basin:Discovery and significance[J]. Acta Petrolei Sinica,2011,32(6):915-927.
[6]马立驰,王永诗,吕建波.济阳坳陷下古生界潜山内幕油气藏勘探[J].油气地质与采收率,2004,11(1):26-29.MA Lichi,WANG Yongshi,LJianbo. Exploration on internal pool of buried hill in lower Palaeozoic group of Jiyang Depression[J].Petroleum Geology and Recovery Efficiency, 2004, 11(1):26-29.
[7]王少鹏,杨庆红,郭铁恩,等.渤海海域CF油田古生界碳酸盐岩潜山储层特征[J].大庆石油地质与开发,2014,33(2):16-21.WANG Shaopeng,YANG Qinghong,GUO Tieen,et al. Characteristics of the Paleozoic carbonate buried-hill reservoirs in CF Oilfield of Bohai Sea[J]. Petroleum Geology&Oilfield Development in Daqing,2014,33:(2)16-21.
[8]于海波,王德英,牛成民,等.渤海海域渤南低凸起碳酸盐岩潜山储层特征及形成机制[J].石油实验地质,2015,37(2):150-157.YU Haibo,WANG Deying,NIU Chengmin,et al. Characteristics and formation mechanisms of buried hill carbonate reservoirs in Bonan Low Uplift, Bohai Bay[J]. Petroleum Geology&Experiment,2015,37(2):150-157.
[9]陈丽祥,牛成民,李慧勇,等.渤海湾盆地渤中21-2构造碳酸盐岩储层发育特征及其控制因素[J].油气地质与采收率,2016,23(2):16-21.CHEN Lixiang,NIU Chengmin,LI Huiyong,et al. Carbonate reservoir characteristics and its controlling factors in Bozhong 21-2Structure,Bohai Bay Basin[J]. Petroleum Geology and Recovery Efficiency,2016,23(2):16-21.
[10]王粤川,韦阿娟,高坤顺,等.渤海海域沙垒田凸起西北部奥陶系碳酸盐岩储层发育主控因素与分布预测[J].海相油气地质,2016,21(2):13-21.WANG Yuechuan,WEI Ajuan,GAO Kunshun,et al. Development controlling factors and distribution predication of Ordovician carbonate reservoirs in the northwestern part of Shaleitian Arch,Offshore Bohai Sea[J]. Marine Origin Petroleum Geology,2016,21(2):13-21.
[11]赵国祥,王清斌,杨波,等.渤中凹陷奥陶系深埋环境下碳酸盐岩溶蚀成因分析[J].天然气地球科学,2016,27(1):111-120.ZHAO Guoxiang,WANG Qingbin,YANG Bo,ea al. Dissolution mechanism analysis of Ordovician carbonates under burial environment of Bozhong Sag,Bohai Sea area[J]. Natural Gas Geoscience,2016,27(1):111-120.
[12]金之钧,朱东亚,胡文瑄,等.塔里木盆地热液活动地质地球化学特征及其对储层影响[J].地质学报,2006,80(2):245-254.JIN Zhijun,ZHU Dongya,HU Wenxuan,et al. Geological and geochemical signatures of hydrothermal activity and their influence on carbonate reservoir beds in the Tarim Basin[J]. Acta Geologica Sinica,2006,80(2):245-254.
[13]朱松柏,王洪峰,王胜军,等.玉北地区深部热液活动的发现及其储层改造意义[J].岩性油气藏,2016,28(3):42-47.ZHU Songbai,WANG Hongfeng,WANG Shengjun,et al. Hydrothermal activities of Ordovician and its significance for alteration to carbonate reservoirs in Yubei area[J]. Lithologic Reservoirs,2016,28(3):42-47.
[14]田雷,崔海峰,冯晓军,等.麦盖提斜坡奥陶系热液溶蚀流体对内幕白云岩储层的改造作用[J].石油与天然气地质,2015,36(3):402-408.TIAN Lei,CUI Haifeng,FENG Xiaojun,et al. Reconstruction effect of the Ordovician hydrothermal dissolution fluid on interior dolomite reservoirs in Maigaiti Slope,Tarim Basin[J]. Oil&Gas Geology,2015,36(3):402-408.
[15]李忠,黄思静,刘嘉庆,等.塔里木盆地塔河奥陶系碳酸盐岩储层埋藏成岩和构造—热流体作用及其有效性[J].沉积学报,2010,28(5):969-979.LI Zhong,HUANG Sijing,LIU Jiaqing,et al. Buried diagenesis,structurally controlled thermal-fluid process and their effect on Ordovician Carbonate Reservoirs in Tahe,Tarim Basin[J]. Acta Sedimentologica Sinica,2010,28(5):969-979.
[16]李辉,李国蓉,罗韵,等.塔河地区奥陶系碳酸盐岩储层深部热液特征分析[J].东北石油大学学报,2014,38(6):12-23.LI Hui,LI Guorong,LUO Yun,et al. Buried Diagenesis,Analysis of characteristics of deep hydrothermal fluids in Ordovician carbonate reservoir in Tahe area[J]. Journal of Northeast Petroleum University,2014,38(6):12-23.
[17]朱东亚,金之钧,孙冬胜,等.南方震旦系灯影组热液白云岩化及其对储层形成的影响研究:以黔中隆起为例[J].地质科学,2014,49(1):161-175.ZHU Dongya,JIN Zhijun,SUN Dongsheng,et al. Hydrothermal dolomitization of Dengying Formation of Sinian in South China and its effect on reservoir formation:An example from Qianzhong Uplift[J]. Chinese Journal of Geology,2014,49(1):161-175.
[18]杨海军,李开开,潘文庆,等.塔中地区奥陶系埋藏热液溶蚀流体活动及其对深部储层的改造作用[J].岩石学报,2012,28(3):783-792.YANG Haijun,LI Kaikai,PAN Wenqing,et al. Burial hydrothermal dissolution fluid activity and its transforming effect on the reservoirs in Ordovician in Central Tarim[J]. Acta Petrologica Sinica,2012,28(3):783-792.
[19]李大伟.新构造运动与渤海湾盆地上第三系油气成藏[J].石油与天然气地质,2004,25(2):170-175.LI Dawei. Neotectonism and Neogene oil and gas pools in Bohai Bay Basin[J]. Oil&Gas Geology,2004,25(2):170-175.
[20]董月霞,周海民,夏文臣.南堡凹陷火山活动与裂陷旋回[J].石油与天然气地质,2000,21(4):24-27.DONG Yuexia, ZHOU Haimin, XIA Wenchen. Volcanic activities and rift-subsidence cycles in Nanpu Sag[J]. Oil&Gas Geology,2000,21(4):24-27.
[21]金之钧,胡文瑄,张刘平,等.深部流体活动及油气成藏效应[M].北京:科学出版社,2007:40-53.JIN Zhijun,HU Wenxuan,ZHANG Liuping,et al. Deep fluid activities and their effectiveness on hydrocarbon generation and accumulation[M]. Beijing:Science Press,2007:40-53.
[22]李庆,胡文瑄,张军涛,等.塔里木盆地西北缘中寒武统硅质岩特征与形成环境[J].矿物学报,2010,30(3):293-303.LI Qing,HU Wenxuan,ZHANG Juntao, et al. Characteristics and formation environment of Middle Cambrian siliconites in Northwestern Margin of Tarim Basin[J]. Acta Mineralogica Sinica,2010,30(3):293-303.
[23]肖波,秦克章,李光明,等.西藏驱龙巨型斑岩Cu-Mo矿床的富S、高氧化性含矿岩浆:来自岩浆成因硬石膏的证据[J].地质学报,2009,83(12):1860-1868.XIAO Bo,QIN Kezhang,LI Guangming, et al. S-rich, highlyoxidized ore-bearing magma in the Qulong giant porphyry-type CuMo deposit in Southern Tibet:Evidence from magmatogenic anhydrite[J]. Acta Geologica Sinica,2009,83(12):1860-1868.
[24]刘丽红,黄思静,王春莲,等.碳酸盐岩中方解石胶结物的阴极发光环带与微量元素构成的关系:以塔河油田奥陶系碳酸盐岩为例[J].海相油气地质,2010,15(1):55-60.LIU Lihong, HUANG Sijing, WANG Chunlian, et al. Cathodoluminescence zonal texture of calcite cement in carbonate rock and its relationship with trace element composition:A case of Ordovician carbonate rock of Tahe Oilfield, Tarim Basin[J].Marine Origin Petroleum Geology,2010,15(1):55-60.
[25]张浩,陈刚,朱玉双,等.柴达木盆地英西地区渐新统热液改造型白云岩的发现与意义[J].地质科技情报,2017,36(1):87-97.ZHANG Hao,CHEN Gang,ZHU Yushuang,et al. Discovery and significance of dolomites altered by hydrothermal fluid in Oligocene reservoirs of the Yingxi Area, Qaidam Basin[J]. Geological Science and Technology Information,2017,36(1):87-97.
[26]黄擎宇.塔里木盆地中央隆起区寒武-奥陶系白云岩化作用及白云岩储层成因研究[D].成都:成都理工大学,2014:48-60.HUANG Qingyu. Dolomitization and origin of the Cambrian-Ordovician dolomite reservoirs in the Central Uplift, Tarim Basin[D]. Chengdu:Chengdu University of Technology,2014:48-60.
[27]杨宁,吕修祥,郑多明.塔里木盆地火成岩对碳酸盐岩储层的改造作用[J].西安石油大学学报(自然科学版),2005,20(4):1-4.YANG Ning,LXiuxiang,ZHENG Duoming. Alteration of the igneous rock on the carbonate reservoir in Tarim Basin[J].Journal of Xi’an Shiyou Universitiy(Natural Science Edition),2005,20(4):1-4.